高纬电离层中非麦克斯韦分布等离子体的非相干散射谱的模拟

使用一个修正的双麦克斯韦分布函数，通过最小均方适应技术使它与高纬电离层Ｆ区中离子的非麦克斯韦速度分布函数相适配．结果表明，使用这样的分布函数可以简化非相干散射谱的计算，并有助于简化高纬地区电离层非相干散射谱的反演．     

Luku Alkali Syenite in the Hongge Ore District, SW China: Geochemistry, Geochronology and Metallogenic Significance

Luku alkali syenite is distributed throughout the southern end of the Hongge basic-ultrabasic intrusion in Panzhihua, Sichuan, SW China. Using LA-ICP-MS, the alkali syenite intrusion yielded a zircon U-Pb age of 264.5 ± 1.6 Ma, concordant with the ages of the E’meishan large igneous province (260 Ma). The intrusion displayed silica-saturated, Al-adequate and alkali-rich signatures, with SiO2 62.07%–64.04%, Al2O3 16.26%–16.79% and Na2O + K2O 9.17%–9.91% (averaging 9.31%). The rock falls into the alkaline zone on the SiO2-A.R. diagram, as well as in the potassium zone on the K2O-Na2O diagram, indicating a potassium alkaline rock. The rock has a low total REE concentration and showed enrichment in LREE (LREE/HREE = 7.06–7.95), typical negative Eu anomalies (δEu = 0.73–0.80), trace element deficiencies in LILEs (Ba, K, Sr, Zr) and enrichment in HFSEs (Th, U, Nd, Sm, Ta and Nb), displaying crust and mantle element information. Zircons show a strong positive Ce anomaly and negative Eu anomaly, similar to the characteristics of crustal source magmatic zircon, however the (Lu/Gd)N ratio ranges from 1.48 to 3.17, and the (Yb/Sm)N ratio ranges from 38.49 to 77.15, which are similar to the characteristics of mantle-derived magmatic zircon. In the La/Yb-δEu correlation diagram, the data plots near the boundary between crust type and crust-mantle type. From the combined ‘trinity’ spatiotemporal relationship of Indosinian intermediate-acid alkali intrusive rocks in the Panxi area with E’meishan basalt and basic-ultrabasic intrusive rocks, the regional tectonic evolution and the partial melting model of the most intraplate magma sources, we believe that the Luku alkali syenite in Sichuan was formed from the partial melting of a crust-mantle source material, due to underplating of the mantle plume basic magma.     

基于城市GPS控制网的航测像控点测量

GPS定位是目前国内外最先进的测量手段之一,以其高精度、高效率、高效益、全天候的优势被广泛用运于我国的经济建设中,本文在徐州市三等GPS网的基础上,探讨了GPS在我市东区航测野外像控点测量中的应用———类星形的布网方案及其平面和拟合高程的精度与可靠性。     

玉树7.1级地震断层地表破裂带应急科考

玉树7.1级地震断层同震地表破裂带由3条主破裂左阶组成,总体走向300°～320°,隆宝镇上见有约2km长的雁列式张裂缝,北侧主破裂长约16km,中间主破裂长约9km,南侧主破裂长约7km,总长约34km。各主破裂均由一系列支破裂雁列组成,支破裂表现为一系列挤压鼓包与张裂缝相间排列或雁列式张裂缝,最南端禅古寺表现为垂直位错。破裂为左旋走滑性质,最大走滑位移量位于北侧主破裂上,约1.8m。     

强雷暴个例云内闪电与上升气流及液水含量关系的三维数值模拟

利用建立的三维闪电数值模式,模拟研究了北京2001年8月23日一次强雷暴发展过程中的云内闪电通道特征及其与上升气流和液水含量（LWC）之间的关系。结果发现：在强雷暴发展过程中,由于雪晶往往在上升气流相对较弱及LWC较低的地方形成、发展,与霰粒子之间的非感应起电过程首先发生在这些区域,然后发生电荷分离。因此,云内闪电往往在上升气流较弱和LWC相对较低的区域触发。闪电触发后,上行先导延伸区域的LWC较小,而下行先导延伸区的LWC取决于强风暴云发展的阶段。强风暴成熟期发生的闪电,下行先导可以延伸到较大LWC区,而无法延伸到LWC最大区。强雷暴衰退期发生的闪电,下行先导可以延伸到LWC最大区。     

某高层建筑桩筏基础桩间土反力原位测试研究

通过对陕西省邮政电信网管中心大楼工程的桩筏基础进行原位测试,分析得到了西北黄土地区高层建筑桩筏基础的沉降特性、桩间土反力分布、桩顶反力分布、桩间土与桩承担竖向荷载的比例,其结果可供实际工程设计及高层建筑结构设计计算理论研究参考。     

A 33 Ma lithostratigraphic record of tectonic and paleoceanographic evolution of the South China Sea

The 853 m thick sediment sequence recovered at ODP Site 1148 provides an unprecedented record of tectonic and paleoceanographic evolution in the South China Sea over the past 33 Ma. Litho-, bio-, and chemo-stratigraphic studies helped identify six periods of changes marking the major steps of the South China Sea geohistory. Rapid deposition with sedimentation rates of 60 m/Ma or more characterized the early Oligocene rifting. Several unconformities from the slumped unit between 457 and 495 mcd together erased about 3 Ma late Oligocene record, providing solid evidence of tectonic transition from rifting/slow spreading to rapid spreading in the South China Sea. Slow sedimentation of 20–30 m/Ma signifies stable seafloor spreading in the early Miocene. Dissolution may have affected the completeness of Miocene–Pleistocene succession with short-term hiatuses beyond current biostratigraphical resolution. Five major dissolution events, D-1 to D-5, characterize the stepwise development of deep water masses in close association to post-Oligocene South China Sea basin transformation. The concurrence of local and global dissolution events in the Miocene and Pliocene suggests climatic forcing as the main mechanism causing deep water circulation changes concomitantly in world oceans and in marginal seas. A return of high sedimentation rate of 60 m/Ma to the late Pliocene and Pleistocene South China Sea was caused by intensified down-slope transport due to frequent sea level fluctuations and exposure of a large shelf area during sea level low-stands. The six paleoceanographic stages, respectively corresponding to rifting (33–28.5 Ma), changing spreading southward (28.5–23 Ma), stable spreading to end of spreading (23–15 Ma), post-spreading balance (15–9 Ma), further modification and monsoon influence (9–5 Ma), and glacial prevalence (5–0 Ma), had transformed the South China Sea from a series of deep grabens to a rapidly expanding open gulf and finally to a semi-enclosed marginal sea in the past 33 Ma.     

Analysis of spectral characteristics among different sensors by use of simulated RS images

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草鱼呼肠孤病毒vp5基因诱饵重组载体的构建、转化与自激活作用检测

根据草鱼呼肠孤病毒(Grass Carp Reovirus,GCRV)的vp5基因设计特异性引物,并扩增其开放阅读框序列(open reading frame,ORF),然后连接至pGBKT7载体上构建酵母双杂交诱饵载体pGBKT7-vp5,转化至酵母菌Y2HGold,并进行PCR鉴定以及自激活性和毒性检测。PCR、酶切以及测序表明,pGBKT7-vp5重组诱饵载体构建成功。自激活性和毒性检测显示,阳性重组菌株pGBKT7-vp5/Y2HGold和阴性对照菌株pGBKT7/Y2HGold在SD/-Trp平板上出现大小相一致的乳白色菌落,且在SD/-Trp/X-α-Gel、SD/-Trp/AbA+/X-α-Gel平板上生长出蓝色菌落,而在SD/-Trp/-Ade/-His无菌落出现。表明重组菌株pGBKT7-vp5/Y2HGold表达的融合蛋白激活了报告基因AUR1-C和MEL1,没有激活报告基因ADE2和HIS3并且对宿主菌无毒性。该重组诱饵载体可用于酵母双杂交系统进一步筛选cDNA文库中与其相互作用的蛋白。     

《从空中看香港图集》正在编制中

中国科学院、香港中文大学新建的地球信息科学联合实验室,正在编制《从空中看香港图集》,以航空与卫星影像、地图和空中与地面照片,反映香港的自然景观,城市发展,显示香港特区同祖国的唇齿相依关系,以及香港在中国和世界中的特殊地位。同以往出版的香港地图集相比,该图集的结构和内容有许多新的特色。